From the
Oregon coast we take OR Hwy 22 eastward. This route takes us through
Salem, the state capitol of Oregon. As we pass over the bridge on the
Willamette River, we see the
Willamette Queen at dock in
Riverfront Park. Another time it'd be fun to take one of their cruises.
We stay on Hwy 22 out of Salem as it follows the north fork of the
Santiam River up into the
Cascades. From the Willamette Valley there are three major routes up into the Cascades:
- Hwy 22 from Salem
- Hwy 20 from Albany/Lebanon
- Hwy 126 from Eugene
Of these three we've found Hwy 22 to be the easiest to drive. All three have beautiful scenery. Hwy 22 runs past the Detroit Dam and Lake. Unlike those in California, all of Oregon's rivers and lakes look pretty full this year.
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North Fork of the Santiam |
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The trees get taller as we climb higher. That night we camp at
Belknap Hot Springs, one of our favorite stops in this neck of the woods (see visits in
once,
twice in 2011 and then again
returning from Alaska in 2012).
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Tall trees along Hwy 22 |
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Camped at Belknap Hot Springs |
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Morning inside van |
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The next morning our first stop is
Larry's RV in Redmond OR since Peter wants to check out a 4x4 camper {sigh}. It has some nice features, but eats considerably more fuel than the
Free Spirit.
We camp at
LaPine State Park along the
Deschutes River. We're delighted to find a campsite along the river banks. It would be fun to raft the Deschutes sometime on another trip - it looks very scenic.
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Deschutes as it flows from the north |
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LaPine campsite |
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Deschutes as it flows to the south |
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During a snack before dinner we have a unexpected guest at our table.
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Hi there - I'm very friendly and very hungry |
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Ooooo nuts - I LOVE nuts |
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Chomp - chomp - chomp |
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In the morning we drive into
Newberry National Volcanic Monument. The caldera itself is over 50 miles wide and contains two lakes - Paulina Lake and East Lake.
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OR Hwy 21 towards Newberry Caldera |
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Entrance to Newberry National Volcanic Monument |
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The salesman at Larry's RV recommended our seeing the Big Obsidian Flow while we're at in the
Newberry Volcano caldera. Both of us love obsidian, so of course we have to see it. The square mile flow is only 1300 years old (young geologically speaking). The flow only is only 10%
obsidian while the rest consists of a mix of grey and black
pumice, which is also a type of volcanic glass.
Why is obsidian black? Tiny black particles of iron oxide act like a drop of black ink in a glass of clear water. To the native tribes in this area obsidian was the same as money in the bank. It was highly valued as a trade item for making tools. In fact, even today obsidian blades are superior to even surgical steel.
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Obsidian rocks in rail wall to stairs |
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View from the top of the flow over Paulina Lake |
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Rain water pond collects below flow |
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Trail through flow |
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Glassy crystals formed in taffy like obsidian |
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Obsidian rocks |
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Large outcropping of obsidian stands out in the flow |
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The day is wearing on and we're decided to make a run for home. So it's time to get back on the road if we want to sleep in our bed at home tonight.
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Big bear sells sporting goods in the Cascades |
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Lumberjack advertizes motel |
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There's the fire in the Trinity Alps |
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Summer hay's stored for winter |
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Mount Shasta's up ahead |
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Recent forest fire |
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Grass Lake |
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We stop at a Vista Point and are treated with an excellent view of Mount Shasta which dominates the surrounding landscape. This large volcanic mountain can be seen from over 100 miles away. It rises 11,000 feet from the base to the summit for a total elevation of 14,162' above sea level. It has a 17 mile diameter with 5 glaciers including the largest one in California.
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Mount Shasta |
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Castle Crags from the north |
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Shasta Lake is still alarmingly low |
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but the Sacramento River looks full. |
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Some farmers are still growing rice in the Central Valley |
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while others just plow dusty fields |
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Late summer in the East Bay hills |
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Full moon rising - we'll be home tonight! |
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